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[PDF] Top 20 CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes from soil of a burned grassland in Central Africa

Has 10000 "CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes from soil of a burned grassland in Central Africa" found on our website. Below are the top 20 most common "CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes from soil of a burned grassland in Central Africa".

CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O fluxes from soil of a burned grassland in Central Africa

CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes from soil of a burned grassland in Central Africa

... 1996). Sub-Saharan Africa grasslands occupy approximately ...millions of km 2 and most of this area is affected by fire (White et ...cover and biodiversity (Menault, 1977; ... See full document

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The European CO&lt;sub&gt;2&lt;/sub&gt;, CO, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O balance between 2001 and 2005

The European CO<sub>2</sub>, CO, CH<sub>4</sub> and N<sub>2</sub>O balance between 2001 and 2005

... Spatial and temporal extent of the component fluxes and stock changes of the European C and GHG ...Component fluxes are expressed in Tg C y −1 for CO ... See full document

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Comparisons of continuous atmospheric CH&lt;sub&gt;4&lt;/sub&gt;, CO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O measurements &amp;ndash; results from a travelling instrument campaign at Mace Head

Comparisons of continuous atmospheric CH<sub>4</sub>, CO<sub>2</sub> and N<sub>2</sub>O measurements &ndash; results from a travelling instrument campaign at Mace Head

... suite of the CRDS systems consists of four cylinders filled with synthetic gas mixture by Deuste Steininger (Mühlhausen, ...GasLab in Jena using ...pressure. In this study we will use hourly ... See full document

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Greenhouse gas emissions (CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O) from perialpine and alpine hydropower reservoirs

Greenhouse gas emissions (CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O) from perialpine and alpine hydropower reservoirs

... Changes in Atmospheric Constituents and Radiative Forcing, in: Climate Change 2007: the physical science basis, Contribution of Working Group I to the Fourth Assessment Report of the ... See full document

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Temporal and spatial variations of soil CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O fluxes at three differently managed grasslands

Temporal and spatial variations of soil CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes at three differently managed grasslands

... tems and the atmosphere is needed to reliably quantify these fluxes and to develop future mitigation ...aged grassland ecosystems, temporal and spatial variabili- ties of these ... See full document

15

Latitude-time variations of atmospheric column-average dry air mole fractions of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O

Latitude-time variations of atmospheric column-average dry air mole fractions of CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O

... Foundation of Research Science and Technology contracts C01X0204 and ...support of the Bialystok and Orl ´eans TCCON sites from the Senate of Bremen and EU projects ... See full document

26

Fluxes of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O from soil of burned grassland savannah of central Africa

Fluxes of CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O from soil of burned grassland savannah of central Africa

... CO 2 than unburned plots during the 1st campaign (one month after burning, dry sea- son) but this difference was not detectable any longer in the 2nd campaign (growing ...effect of fire was ... See full document

38

A satellite data driven biophysical modeling approach for estimating northern peatland and tundra CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; fluxes

A satellite data driven biophysical modeling approach for estimating northern peatland and tundra CO<sub>2</sub> and CH<sub>4</sub> fluxes

... tower CH 4 observations and TCF model simulation results us- ing in-situ information (in parentheses) or MERRA and MODIS ...Measures of relative agreement include Pearson ... See full document

59

Biogeochemical modeling of CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; production in anoxic Arctic
soil microcosms

Biogeochemical modeling of CO<sub>2</sub> and CH<sub>4</sub> production in anoxic Arctic soil microcosms

... procedures, and results for the microcosm tests have been reported previously (Herndon et ...three soil cores were taken from center, ridge, and trough locations in a low-center polygon ... See full document

21

Ten years of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt;, CO and N&lt;sub&gt;2&lt;/sub&gt;O fluxes over Western Europe inferred from atmospheric measurements at Mace Head, Ireland

Ten years of CO<sub>2</sub>, CH<sub>4</sub>, CO and N<sub>2</sub>O fluxes over Western Europe inferred from atmospheric measurements at Mace Head, Ireland

... network of stations in the synthesis inversion of Bousquet et ...monthly fluxes over large regions (Europe being one of them) with a fixed a priori geographic emission pattern within ... See full document

47

N&lt;sub&gt;2&lt;/sub&gt;O, NO, N&lt;sub&gt;2&lt;/sub&gt; and CO&lt;sub&gt;2&lt;/sub&gt; emissions from tropical savanna and grassland of northern Australia: an incubation experiment with intact soil cores

N<sub>2</sub>O, NO, N<sub>2</sub> and CO<sub>2</sub> emissions from tropical savanna and grassland of northern Australia: an incubation experiment with intact soil cores

... representative of many savanna sites found in the region under comparable hygric conditions (see ...2011) and the typical natural fire regime is a fire for 2 out of 3 years (Hutley et ... See full document

19

Decadal variability of soil CO&lt;sub&gt;2&lt;/sub&gt; NO, N&lt;sub&gt;2&lt;/sub&gt;O, and CH&lt;sub&gt;4&lt;/sub&gt; fluxes at the Höglwald Forest, Germany

Decadal variability of soil CO<sub>2</sub> NO, N<sub>2</sub>O, and CH<sub>4</sub> fluxes at the Höglwald Forest, Germany

... Bernhofer, C., Carrara, A., Chevallier, F., De Noblet, N., Friend, A. D., Friedlingstein, P., Grunwald, T., Heinesch, B., Keronen, P., Knohl, A., Krinner, G., Loustau, D., Manca, G., Matteucci, G., Miglietta, F., ... See full document

49

Suitability of quantum cascade laser spectroscopy for CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O eddy covariance flux measurements

Suitability of quantum cascade laser spectroscopy for CH<sub>4</sub> and N<sub>2</sub>O eddy covariance flux measurements

... town of Reeuwijk in the Netherlands (Coord 52 ◦ 01 ′ 15 ′′ N, 4 ◦ 01 ′ 17 ′′ ...area of the measurement loca- tion has soil consisting of a clayey peat or peaty clay layer ... See full document

14

Influence of meteorology and interrelationship with greenhouse gases (CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt;) at a sub-urban site of India

Influence of meteorology and interrelationship with greenhouse gases (CO<sub>2</sub> and CH<sub>4</sub>) at a sub-urban site of India

... concentrations of atmospheric GHGs, with specifications meeting WMO standards of ...nature of the site, flow rateis fixed to be 7 liters per minute (L m −1 ... See full document

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Mapping CH&lt;sub&gt;4&lt;/sub&gt; : CO&lt;sub&gt;2&lt;/sub&gt; ratios in Los Angeles with CLARS-FTS from Mount Wilson, California

Mapping CH<sub>4</sub> : CO<sub>2</sub> ratios in Los Angeles with CLARS-FTS from Mount Wilson, California

... high clouds, data are filtered out when the corresponding SVO oxygen SCD ratio is less than 1 or greater than 1.1. For low clouds, data with retrieved target oxygen SCD devi- ating more than 10 % from the ... See full document

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Chlorine activation by N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;: simultaneous, in situ detection of ClNO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; by chemical ionization mass spectrometry

Chlorine activation by N<sub>2</sub>O<sub>5</sub>: simultaneous, in situ detection of ClNO<sub>2</sub> and N<sub>2</sub>O<sub>5</sub> by chemical ionization mass spectrometry

... dissociate in the CDC so the relative signals detected after the CDC provide only lower limits to the true branching of the ion-molecule reactions occurring upstream of the ...fields of −60 to ... See full document

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Technical note: A stratospheric climatology for O&lt;sub&gt;3&lt;/sub&gt;, H&lt;sub&gt;2&lt;/sub&gt;O, CH&lt;sub&gt;4&lt;/sub&gt;, NO&lt;sub&gt;x&lt;/sub&gt;, HCl and HF derived from HALOE measurements

Technical note: A stratospheric climatology for O<sub>3</sub>, H<sub>2</sub>O, CH<sub>4</sub>, NO<sub>x</sub>, HCl and HF derived from HALOE measurements

... (GCMs) and Chemistry Transport Models (CTMs) need information about the spatial distribution of the chemical composition for some key tracer species, ...vapor, in order to achieve realistic results ... See full document

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Chlorine activation by N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;: simultaneous, in situ detection of ClNO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; by chemical ionization mass spectrometry

Chlorine activation by N<sub>2</sub>O<sub>5</sub>: simultaneous, in situ detection of ClNO<sub>2</sub> and N<sub>2</sub>O<sub>5</sub> by chemical ionization mass spectrometry

... housed in a perforated stainless steel tube capped with entrance and exit lenses, and are followed by an off-axis electron multiplier detector with dynode from Extrel ...pulses of the ... See full document

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Rate coefficients for the reaction of methylglyoxal (CH&lt;sub&gt;3&lt;/sub&gt;COCHO) with OH and NO&lt;sub&gt;2&lt;/sub&gt; and glyoxal (HCO)&lt;sub&gt;2&lt;/sub&gt; with NO&lt;sub&gt;3&lt;/sub&gt;

Rate coefficients for the reaction of methylglyoxal (CH<sub>3</sub>COCHO) with OH and NO<sub>2</sub> and glyoxal (HCO)<sub>2</sub> with NO<sub>3</sub>

... formation of PAN, which is potentially much longer lived and can be transported longer distances and, therefore, impact atmospheric chemistry in remote ...yield from this degra- dation ... See full document

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Consistency and quality assessment of the Metop-A/IASI and Metop-B/IASI  operational trace gas products (O&lt;sub&gt;3&lt;/sub&gt;,  CO,  N&lt;sub&gt;2&lt;/sub&gt;O,   CH&lt;sub&gt;4&lt;/sub&gt;, and  CO&lt;sub&gt;2&lt;/sub&gt;) in the subtropical North Atlantic

Consistency and quality assessment of the Metop-A/IASI and Metop-B/IASI operational trace gas products (O<sub>3</sub>, CO, N<sub>2</sub>O, CH<sub>4</sub>, and CO<sub>2</sub>) in the subtropical North Atlantic

... consistent, and high-quality long-term monitor- ing of the composition of the atmosphere is fundamental for addressing the challenges of climate ...research. In this con- text ... See full document

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